首页|基于复经验正交函数的日本以南黑潮路径时空变化特征及其因果关系研究

基于复经验正交函数的日本以南黑潮路径时空变化特征及其因果关系研究

Spatiotemporal variation characteristics and causal relationship of the Kuroshio path south of Japan based on complex empirical orthogonal functions

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日本以南黑潮路径变化的相关分析一直是热点之一.过去的研究指出日本以南黑潮路径变化受到多种因素的影响,如上游流量、中尺度涡旋、气候信号等.然而,关于这些影响因素之间的相互因果关系尚不完全清楚.本文基于50a(1958-2007年)中国海洋再分析数据集(CORA)和14a(2008-2021年)卫星高度计资料,获取了日本以南黑潮路径时间序列,并利用复经验正交函数(CEOF)分析方法对其进行时空特征分析.结果表明,经CEOF分析获取的前两个主模态可以描述日本以南黑潮路径时空变化的主要特征,且分别代表与之相关的东传和西传信号.进一步地,基于信息流理论的因果分析结果表明:一方面,太平洋十年涛动(PDO)通过风应力的变化影响副热带逆流(STCC)区域的涡旋活动,从而影响吐噶喇海峡的黑潮输运变化,进而对东传信号产生直接影响,最终影响日本以南海域的黑潮路径变化;另一方面,黑潮延伸体的涡旋活动受到北太平洋涡旋振荡(NPGO)的影响,促使该区域的中尺度涡旋向西移动,进而对西传信号产生直接影响,最终影响日本以南海域的黑潮路径变化.此外,分析结果还表明:日本以南海域的相对涡度和再循环流强度变化是对黑潮路径变化的响应,而非影响黑潮路径变化的因素.
The analysis of the changes in the path of the Kuroshio south of Japan has always been a hot topic.Previ-ous studies have pointed out that the changes in the Kuroshio path south of Japan are influenced by various factors,such as upstream transport,mesoscale eddies,climate signals etc.However,the causal relationship between these influencing factors is not fully understood.The paper first obtains the time series of the Kuroshio path south of Ja-pan based on the 50 year(1958-2007)China Ocean Reanalysis dataset(CORA)and 14 year(2008-2021)satellite altimeter data,and uses the Complex Empirical Orthogonal Function(CEOF)analysis method to analyze its spati-otemporal characteristics.The results show that the first two main modes obtained by CEOF analysis can describe the main characteristics of the space-time variation of the Kuroshio path in the south of Japan and represent the re-lated eastward and westward signals,respectively.Furthermore,the causal analysis results based on information flow theory indicate that:on the one hand,PDO affects the eddy kinetic energy in the subtropical countercurrent(STCC)region through changes in wind stress,thus affecting the changes of Kuroshio transport in the Tokara Strait,and then has a direct impact on the eastward signal,and finally affects the changes of the Kuroshio path in the southern region of Japan.On the other hand,the eddy kinetic energy of the Kuroshio extension is influenced by the NPGO signal,which affects the westward movement of the mesoscale eddies in the region,thereby directly af-fecting the westward signal and ultimately affecting the Kuroshio path changes in the region south of Japan.In addi-tion,the experimental results also indicate that the relative vorticity and recirculation gyre strength in the southern region of Japan are responses to the changes in the Kuroshio path,rather than factors affecting the changes in the Kuroshio path.

Kuroshio path south of JapanCEOFcausality analysisinformation flow

纪增华、武晓博、李威、曹力戈、张蒙蒙、董婉秋、韩桂军

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天津大学海洋科学与技术学院天津市海洋环境与安全保障重点实验室,天津 300072

国家海洋技术中心,天津 300112

国家海洋环境预报中心,北京 100081

日本以南黑潮路径 复经验正交函数 因果分析 信息流

国家重点研发计划国家自然科学基金国家自然科学基金

2023YFC31078004237619041876014

2024

海洋学报(中文版)
中国海洋学会

海洋学报(中文版)

CSTPCD北大核心
影响因子:1.044
ISSN:0253-4193
年,卷(期):2024.46(8)
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